High pressure phase transformations in aragonite-type carbonates

Abstract

 High-temperature and high-pressure experiments conducted in a diamond-anvil cell revealed phase transformations in the aragonite-type carbonates of strontianite (SrCO₃), cerussite (PbCO₃), and witherite (BaCO₃) at pressures below 4 GPa and ∼1000 °C. The powder X-ray diffraction patterns of these high-pressure phases can be reasonably indexed with the same type of orthorhombic cell having a space group of P2₁22 (17). By assuming 16 MCO₃ (M=Sr, Ba or Pb) molecules in a unit cell, the transition from the aragonite form to a new phase was concomitant with a volume contraction of 4.23, 2.38, and 2.34% for SrCO₃, PbCO₃, and BaCO₃, respectively. If the same phase transition were to occur in CaCO₃, it has been estimated that the transition would accompany a 7% volume contraction.